Spinel Mineral

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A Spinel Mineral is a mineral that belongs to the spinel group and crystallizes in the cubic crystal system.

  • Context:
    • It can occur as the magnesium/aluminium member of the spinel group with the formula MgAl₂O₄.
    • It can form pointed, octahedral crystals, leading to its name derived from the Latin "spina" (meaning spine).
    • It can range in color from colorless to vibrant shades such as red, blue, green, and violet due to trace element substitutions.
    • It can be found in metamorphic rocks, in association with limestone and dolomite, as well as in placer deposits.
    • It can exhibit high refractive indices and hardness (7.5–8 on the Mohs scale), making it suitable for use as a gemstone.
    • It can serve as a geochemical indicator in petrological studies due to its stability under varying pressure and temperature conditions.
    • It can include natural and synthetic variants, with synthetic spinels often used in industrial applications.
    • ...
  • Example(s):
    • Red Spinel, which is known for its vivid red color often mistaken for ruby.
    • Blue Spinel, which is prized for its rare cobalt-colored hues.
    • Synthetic Spinel, which is used in optical materials and as durable coatings in technology.
    • Hercegovinaite, a manganese-dominant spinel variety.
    • ...
  • Counter-Example(s):
    • Garnets, which lack a cubic crystal structure but may also be used as gemstones.
    • Corundums, which have a different chemical composition and crystal structure but share some gemstone qualities.
    • Peridots, which are also magnesium-rich minerals but belong to the olivine group.
  • See: Cubic Crystal System, Oxide Minerals, Spinel Group, H–M Symbol, Magnesium, Aluminium.


References

2024

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